Abstract
SummaryPore size distributions obtained from the relationship between moisture content and suction are not dependable in fine‐textured soils because of shrinkage. To overcome this problem, methods such as nitrogen sorption, mercury intrusion porosimetry, non‐polar liquid desorption and thin sectioning have been used. In order to pre‐dry samples without changes in the pore system, freeze‐drying, organic liquid replacement of soil water, and critical point drying techniques have been employed. These methods of soil drying and pore size measurement are described and compared, and the validity of their use in soil studies is examined. The measurement of pore sizes by water desorption is also discussed.
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